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176 results for “evaporation”
Datasets for "Peatland evaporation across hemispheres: contrasting controls and sensitivity to climate warming driven by plant functional types" - Version 2
<p>Version 2 of datasets used for analyses in the paper titled "Peatland evaporation across hemispheres: contrasting controls and sensitivity to climate warming driven by plant functional types" submitted to Biogeosciences. There are two datasets - one from Kopuatai bog, Aotearoa New Zealand, and one from Mer Bleue bog, Canada - which contain gap-filled and filtered data that were used to produce the results of our study.</p> <p>Due to improvements made to our methodology following the paper peer review process, the data in this version slightly differs from that of the previous version. Information on these revisions can be found in the README file below or the Discussion/Peer Review tab of our paper.</p> <p> </p> <p> </p>
Datasets for the article "Evaporative controls on Antarctic precipitation: an ECHAM6 model study using innovative water tracer diagnostics"
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Data for the paper "Dispersion of particles in a sessile droplet evaporating on a heated substrate"
<p><span><span>This file contains the data generated for each case demonstrated in the paper titled "Dispersion of particles in a sessile droplet evaporating on a </span>heated substrate" <br>Authors: Aman Kumar Jain, Fabian Denner, and Berend van Wachem. <br><br>The repository contains the 7 folders for 7 cases performed in stage 2 of the simulation described in table 4 of the paper. Cases C1 and C2 involve a droplet on a substrate at Ts = 25 ◦ C, while C3 and C4 involve a substrate at Ts = 50 ◦C. Marangoni stresses are considered in the even-numbered cases and neglected in the odd-numbered ones. The case names ending with suffix S denotes the standard silica particles and the case names ending with suffix N denotes neutrally buoyant articles. <br></span></p> <p><span>Along with these folders a python script "ParticleCombined.py" is added which uses the particle position data in each case folder to calculate the particle surface density. <br><br>Each case folder contains: <br>The fluid fields, mesh, and particle information are stored in folders Fields, DMs, Meshes and Particles. <br>A .xmf wrapper file is provided to read the simulation results in Paraview. <br>The "results.xmf" file shows the fluid data such as velocity, pressure and liquid volume fraction. The liquid volume fraction value, alpha, tracks the interface of an evaporating sessile droplet. <br>The "results_DEM.xmf" shows the particle data such as the position, velocity and other data sets associated with the particles. <br><br>Each case folder contains five *.csv files which contain the information of particle position for 5-time instances and are processed using the python script "ParticleCombined.py". <br><br>This research was funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation), grant number 452916560.<br></span></p>
Datasets and code of the manuscript 'Insights into the Aerodynamic versus Radiometric Surface Temperature Debate in Thermal-based Evaporation Modeling'
<p>This contains the datasets and codes that were used to generate the results and discussions in the manuscript</p>
Additional data for Insights for the Partitioning of Ecosystem Evaporation and Transpiration in Short-Statured Croplands
<p>Data includes LAI and SPA-Crop model outputs for the 2018-2019 winter wheat and for the 2019-2020 winter barley crop seasons.<br> Eddy covariance and meteorological data from Oensingen (CH-Oe2) are available at http://www.europe-fluxdata.eu/home/site-details?id=CH-Oe2</p>
Cutaneous Evaporative Water Loss in Lizards is Variable across Body Regions and Plastic in Response to Humidity
<p>Data and code associated with the 2022 publication in Herpetologica (doi:10.1655/Herpetologica-D-21-00030.1).</p>
NMR_T2_evaporation-of-water_porous-media
<p>Nuclear magnetic resonance (NMR) transversal relaxation time T2 during evaporation of water from porous media was collected. Both homogeneous and inhomogeneous porous media was applied in experiments. Homogeneous porous media was made of uniform-sized glass beads with diameter at either 25 μm or 150 μm. Inhomogeneous porous media included two parts with top and bottom part made of fine and coarse beads respectively. By adjusting the proportion of each part, multiple inhomogeneous porous media was made. The temperature during experiment was controlled at 50 °C and T2 data was recorded every 30 minutes (individual experiment lasted from 3 to 5 days). Carr-Purcell-Meiboom-Gill (CPMG) sequence was applied in data recording and parameters were set at TE=0.2 ms and NECH=18000. Each recording collects 5000 pairs of T2 and corresponding signal amplitude, based on which the transient water content and distribution could be obtained.</p>
Quantifying Salt Crystallization Impact on Evaporation Dynamics from Porous Surfaces
<p>The file contains cumulative evaporative mass losses during evaporation from sand columns saturated with 10%, 15%, and 20% NaCl solutions (mass basis).</p>
Data from: Water availability and temperature as modifiers of evaporative water loss in tropical frogs
<p>Water plays a notable role in the ecology of most terrestrial organisms due to the risks associated with water loss. Specifically, water loss in terrestrial animals happens through evaporation across respiratory tissues or epidermis. Amphibians are ideal systems for studying how abiotic factors impact water loss since their bodies often respond quickly to environmental changes. While the effect of temperature on water loss is well known across many taxa, we are still learning how temperature in combination with humidity or water availability affects water loss. Here, we tested how standing water sources (availability) and temperature (26 and 36°C) together affect water loss in anuran amphibians using a Bayesian framework. We also present a conceptual model for considering how water availability and temperature may interact, resulting in body mass changes. After accounting for phylogenetic and time autocorrelation, we determined how different variables (water loss and uptake rates, temperature, and body size) affect body mass in three species of tropical frogs (<em>Rhinella marina</em>, <em>Phyllobates terribilis</em>, and <em>Xenopus tropicalis</em>). We found that all variables impacted body mass changes with greater similarities between <em>P. terribilis</em> and <em>X.</em> <em>tropicalis</em>, but only temperature showed a notable effect in <em>P. terribilis</em>. Furthermore, we describe how the behavior of <em>P. terribilis</em> might affect its water budget. This study shows how organisms might manage water budgets across different environments and is important for developing our models of evaporative water loss and species distributions.</p>
Flexibility of cutaneous evaporative water loss in response to hydration in pregnant Prairie Rattlesnakes and their neonates
<p>Data and code associated with the paper published in the Journal of Experimental Biology in 2025.</p>
A grid of mass loss rates from catestrophically evaporating rocky planets
<p>The code and data associated with the paper "Dust formation in the outflows of catastrophically evaporating planets" by Booth, Owen & Schulik (2023).</p> <p>Contains:</p> <ul> <li>aiolos.tar.gz: The code used to generate the models</li> <li>mass_loss_grid.tar.gz: The grid of mass-loss rates from planets of different masses and surface temperatures. Note the mass-loss rates are computed assuming the stellar properties of Kepler-1520.</li> </ul> <p> </p> <p> </p>
Water retention curve measurement (evaporation + dew point method)
<p>Experimental video series: measurement of the water retention curve with evaporation method (HYPROP), and dew point (WP4C). Explanation of laboratory methodology for measuring soil hydraulic properties. English and Spanish subtitles.</p> <p>Video serie experimental: medición de la curva de retención de agua con método de evaporación (HYPROP), y punto de rocío (WP4C). Explicación metodología en laboratorio para medición de propiedades hidráulicas del suelo. Subtítulos en Inglés y en Español</p>
Continuous increase in evaporative demand shortened the growing season of European ecosystems in the last decade
<p><strong>Datasets provided above are processed data during the conducting analysis for our paper entitled "Continuous increase in evaporative demand shortened the growing season of European ecosystems in the last decade". </strong></p> <p><strong>Here is the abstract of the paper: </strong></p> <p><strong>Despite previous reports on European growing seasons lengthening due to global warming, evidence shows that this trend has been reversing in the past decade due to increased transpiration needs. We used an innovative method along with space-based observations to determine the timing of greening and dormancy and then to determine existing trends and causes. Early greening still occurs, albeit at slower rates than before. However, a recent (2011-2020) shift in the timing of dormancy has caused the season length to decrease back to 1980s levels. This shortening of season length is attributed primarily to higher atmospheric water demand in summer that suppresses transpiration even for soil moisture levels as of previous years. Transpiration suppression implies that vegetation is unable to meet the high transpiration needs. Our results have implications for future management of European ecosystems (e.g., net carbon balance and water and energy exchange with atmosphere) in a warmer world.</strong></p> <p> </p> <p> </p>
Strong HONO Emissions from Dew and Guttation Evaporation Trigger Severe Photochemical Pollution Formation
<p>Data for the manuscript "Strong HONO Emissions from Dew and Guttation Evaporation Trigger Severe Photochemical Pollution Formation" by Xu et al.</p>
Wet surface evaporation with FLUXNET data
<p>FLUXNET data from 171 stations and software to process it for use in the complementary relationship of evaporation. This repo is intended to allow users to reproduce the analyses from manuscript under review in the journal HESS (Hydrology and Earth System Science). The software and the csv files for 171 stations are included. All data files were obtained from the fluxnet.org web site. Files are all csv. Fluxnet files contain the daily (filename contains "DD") and monthly (filename contains, "MM") average flux data. Sensible and latent heat fluxes are from eddy covariance measurements.</p> <p>The goal of the project is to gain insight into the meaning of the Priestley-Taylor wet-surface evaporation parameter alpha. Four hypotheses regarding how to estimate alpha are proposed in the manuscript.</p> <p>The manuscript (still under review) describing the study in detail is at <a href="https://egusphere.copernicus.org/preprints/2022/egusphere-2022-712/egusphere-2022-712.pdf">https://egusphere.copernicus.org/preprints/2022/egusphere-2022-712/egusphere-2022-712.pdf</a></p> <p>Co-authors on the paper are R. Crago, J. Szilagyi and R. J. Qualls</p> <p>Software was written by R. Crago</p> <p>I will update the link if the paper gets accepted.</p> <p>Instructions: The Python code is in the 'Wet_surface_evap_public.ipynb' file. The other uploaded files contain data. The data should be placed in a suitable folder, and the code in the first few cells should be modified so that the code looks into the directory in which your data are stored. This runs well in Google's Colab environment. The data files and the ipynb file can be uploaded to your google drive. The ipynb file is already in the form of a Jupyter notebook, which is what Colab uses.</p>
Global LAke Surface water Temperature (GLAST): Global lakes are warming slower than surface air temperature due to accelerated evaporation
<p>This repository houses a dataset, known as the Global LAke Surface water Temperature (GLAST), which provides both temporal and spatial details at high resolution for 92,245 lakes worldwide during the period of 1981-2099, with 36% of them situated in Arctic regions. The dataset was established based on four decades (1982-2020) of Landsat satellite images and a physical model (FLake). For a comprehensive overview of the dataset's production methodology, please refer to the paper titled 'Global lakes are warming slower than surface air temperature due to accelerated evaporation' (Tong et al., 2023, Nature Water). Detailed information regarding each data file can be found in the 'readme.docx' file.</p>
Model output data to "Land surface modeling in the Himalayas: on the importance of evaporative fluxes for the water balance of a high elevation catchment"
<p>We provide i) gridded initial conditions (.tif), ii) modeled gridded monthly outputs (.tif), and iii) modeled hourly outputs at the station locations (.txt) for the hydrological year 2019. Information about the variables and units can be found in the figures (.png) associated to each dataset. Details about the datasets can be found in the original publication by Buri and others (2023).</p><p> </p><p>Buri, P., Fatichi, S., Shaw, T. E., Miles, E. S., McCarthy, M. J., Fyffe, C. L., ... & Pellicciotti, F. (2023). Land Surface Modeling in the Himalayas: On the Importance of Evaporative Fluxes for the Water Balance of a High‐Elevation Catchment. <i>Water Resources Research</i>, <i>59</i>(10), e2022WR033841. DOI: <a href="https://doi.org/10.1029/2022WR033841"><strong>10.1029/2022WR033841</strong></a></p>
A Multicenter Study Evaluating AZR-MD-001 in Patients With Meibomian Gland Dysfunction and Evaporative Dry Eye Disease (DED)
ClinicalTrials.gov study NCT03652051. IPD Sharing: NO. Countries: 3. Publications: 1.
Controlled Adverse Environment: A Pilot Study to Evaluate Tear Film Stability and Tear Evaporation
ClinicalTrials.gov study NCT01448356. IPD Sharing: Not stated. Countries: 1. Publications: 2.
Data from: Snake oil in action: Geographic and seasonal variability in epidermal lipids shape evaporative water loss in snakes
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